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Gabbro (pronounced /ˈɡæbroʊ/) refers to a large group of dark, coarse-grained, intrusive mafic igneous rocks chemically equivalent to basalt. Gabbro is dense, greenish or dark-colored and contains pyroxene, plagioclase, amphibole, and olivine (olivine gabbro when olivine is present in a large amount). — “Gabbro - Wikipedia, the free encyclopedia”, en.wikipedia.org
These intrusions formed a sill some 16 km thick, primarily of gabbro, but with significant amounts of anorthosite and other related granitic rocks. The Duluth Complex is one of the largest intrusions of gabbro on earth, and one of the largest layered mafic intrusions known. — “Duluth Complex - Wikipedia, the free encyclopedia”, en.wikipedia.org
Gabbro is part of WikiProject Geology, an attempt at creating a standardized, informative, The first sentence under the Petrology section makes no sense to me: "Gabbro is an extrusive melting lava." Gabbro is an intrusive rock type, not extrusive, and would form from magma rather. — “Talk:Gabbro - Wikipedia, the free encyclopedia”, en.wikipedia.org